Raman spectroscopy of carbonaceous material (RSCM) is frequently used to determine metamorphic peak temper-atures from the structural order of carbonaceous material enclosed in metasediments. This method provides a quick, robust and relatively cheap geothermometer. However, the comparability of the RSCMparameter is low as there are at least three major sources of biasing factors. These sources are the spectral curve-fitting procedure, the sample char-acteristics itself and the experimental design including the used Raman system. To assess the impacts of the biasing factors on RSCM, a series of experiments was performed. The experiments showed that curve-fitting is strongly influenced by individual operator-bias and the degrees of freedom in...
International audienceUnderstanding the thermal evolution of rocks is a key parameter to reconstruct...
Carbonaceous materials (CMs) have been widely used to assess temperatures in sedimentary and metamor...
International audienceThe knowledge of the thermal history of rocks is a key point for reconstructin...
International audienceThe Raman Spectroscopy of Carbonaceous Materials (RSCM) geothermometry approac...
International audienceThe study of the maturity of CM provides a relatively precise tool to estimate...
Metamorphic processes can transform the organic matter in sedimentary rocks into structurally organi...
Raman spectroscopy is an irreplaceable method for chemical and structural characterization of many s...
The degree of crystallinity of amorphous carbonaceous material (CM) increases with heating. Previous...
The Northern Range of Trinidad is a mountain range located along the northern Trinidadian coast form...
These data published in this repository are associated with a paper focused on the Eastern Pyrenees....
To investigate the thermal evolu-tion of foreland basins, many classical methods includ-ing clay min...
International audienceThe Raman Spectroscopy of Carbonaceous Materials (RSCM) permits to quantify th...
International audienceThe occurrence of deposits hosted by carbonaceous materials-rich metasediments...
International audienceGeothermometers based on Raman spectrometry of carbonaceous matter and coverin...
Acknowledgements This work was funded by the School of Geosciences, University of Aberdeen. Stimulat...
International audienceUnderstanding the thermal evolution of rocks is a key parameter to reconstruct...
Carbonaceous materials (CMs) have been widely used to assess temperatures in sedimentary and metamor...
International audienceThe knowledge of the thermal history of rocks is a key point for reconstructin...
International audienceThe Raman Spectroscopy of Carbonaceous Materials (RSCM) geothermometry approac...
International audienceThe study of the maturity of CM provides a relatively precise tool to estimate...
Metamorphic processes can transform the organic matter in sedimentary rocks into structurally organi...
Raman spectroscopy is an irreplaceable method for chemical and structural characterization of many s...
The degree of crystallinity of amorphous carbonaceous material (CM) increases with heating. Previous...
The Northern Range of Trinidad is a mountain range located along the northern Trinidadian coast form...
These data published in this repository are associated with a paper focused on the Eastern Pyrenees....
To investigate the thermal evolu-tion of foreland basins, many classical methods includ-ing clay min...
International audienceThe Raman Spectroscopy of Carbonaceous Materials (RSCM) permits to quantify th...
International audienceThe occurrence of deposits hosted by carbonaceous materials-rich metasediments...
International audienceGeothermometers based on Raman spectrometry of carbonaceous matter and coverin...
Acknowledgements This work was funded by the School of Geosciences, University of Aberdeen. Stimulat...
International audienceUnderstanding the thermal evolution of rocks is a key parameter to reconstruct...
Carbonaceous materials (CMs) have been widely used to assess temperatures in sedimentary and metamor...
International audienceThe knowledge of the thermal history of rocks is a key point for reconstructin...